globalchange  > 过去全球变化的重建
DOI: 10.1007/s00382-011-1129-7
Scopus记录号: 2-s2.0-84866398113
论文题名:
Recent and future sea surface temperature trends in tropical pacific warm pool and cold tongue regions
作者: An S.-I.; Kim J.-W.; Im S.-H.; Kim B.-M.; Park J.-H.
刊名: Climate Dynamics
ISSN: 9307575
出版年: 2012
卷: 39, 期:6
起始页码: 1373
结束页码: 1383
语种: 英语
英文摘要: Using coral data, sea surface temperature (SST) reanalysis data, and Climate Model Intercomparison Project III (CMIP3) data, we analyze 20th-century and future warm pool and cold tongue SST trends. For the last 100 years, a broad La Nina-like SST trend, in which the warming trend of the warm pool SST is greater than that of the cold tongue SST, has appeared in reanalysis SST data sets, 20C scenario experiments of the CMIP3 data and less significantly in coral records. However, most Coupled General Circulation Models subjected to scenarios of future high greenhouse gas concentrations produce larger SST warming trends in cold tongues than in warm pools, resembling El Nino-like SST patterns. In other words, warmer tropical climate conditions correspond to stronger El Nino-like response. Heat budget analyses further verify that warmer tropical climates diminish the role of the ocean's dynamic thermostat, which currently regulates cold tongue temperatures. Therefore, the thermodynamic thermostat, whose efficiency depends on the mean temperature, becomes the main regulator (particularly via evaporative cooling) of both warm pool and cold tongue temperatures in future warm climate conditions. Thus, the warming tendency of the cold tongue SST may lead that of the warm pool SST in near future. © 2011 Springer-Verlag.
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资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/55190
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作者单位: Department of Atmospheric Sciences, Yonsei University, Seoul 120-742, South Korea; APEC Climate Center, Pusan, South Korea; Korea Polar Research Institute, KORDI, Incheon, South Korea

Recommended Citation:
An S.-I.,Kim J.-W.,Im S.-H.,et al. Recent and future sea surface temperature trends in tropical pacific warm pool and cold tongue regions[J]. Climate Dynamics,2012-01-01,39(6)
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